Australian Research Council Centre of Excellence for Coral Reef Studies, James Cook University, Townsville, Queensland, Australia.
College of Science and Engineering, James Cook University, Townsville, Queensland, Australia.
Nature. 2018 Apr;556(7702):492-496. doi: 10.1038/s41586-018-0041-2. Epub 2018 Apr 18.
Global warming is rapidly emerging as a universal threat to ecological integrity and function, highlighting the urgent need for a better understanding of the impact of heat exposure on the resilience of ecosystems and the people who depend on them . Here we show that in the aftermath of the record-breaking marine heatwave on the Great Barrier Reef in 2016 , corals began to die immediately on reefs where the accumulated heat exposure exceeded a critical threshold of degree heating weeks, which was 3-4 °C-weeks. After eight months, an exposure of 6 °C-weeks or more drove an unprecedented, regional-scale shift in the composition of coral assemblages, reflecting markedly divergent responses to heat stress by different taxa. Fast-growing staghorn and tabular corals suffered a catastrophic die-off, transforming the three-dimensionality and ecological functioning of 29% of the 3,863 reefs comprising the world's largest coral reef system. Our study bridges the gap between the theory and practice of assessing the risk of ecosystem collapse, under the emerging framework for the International Union for Conservation of Nature (IUCN) Red List of Ecosystems , by rigorously defining both the initial and collapsed states, identifying the major driver of change, and establishing quantitative collapse thresholds. The increasing prevalence of post-bleaching mass mortality of corals represents a radical shift in the disturbance regimes of tropical reefs, both adding to and far exceeding the influence of recurrent cyclones and other local pulse events, presenting a fundamental challenge to the long-term future of these iconic ecosystems.
全球变暖正在迅速成为对生态完整性和功能的普遍威胁,凸显出急需更好地了解热暴露对生态系统弹性以及依赖这些生态系统的人类的影响。在这里,我们表明,在 2016 年大堡礁创纪录的海洋热浪之后,珊瑚在累积热暴露超过关键阈值度加热周(3-4°C 周)的珊瑚礁上立即开始死亡。八个月后,暴露于 6°C 周或更长时间导致了珊瑚生物群组成的前所未有的区域规模转变,反映出不同分类群对热应激的明显不同的反应。快速生长的鹿角珊瑚和板状珊瑚大量死亡,使构成世界上最大珊瑚礁系统的 3863 个珊瑚礁中的 29%的三维结构和生态功能发生了变化。我们的研究通过严格定义初始状态和崩溃状态、确定主要变化驱动因素以及建立定量崩溃阈值,在评估生态系统崩溃风险的理论和实践之间架起了桥梁,这是根据国际自然保护联盟(IUCN)生态系统红色名录的新兴框架进行的。珊瑚白化后大量死亡的现象越来越普遍,这标志着热带珊瑚礁的干扰机制发生了根本性转变,既增加了又远远超过了周期性飓风和其他局部脉冲事件的影响,对这些标志性生态系统的长期未来构成了根本性挑战。